Structure, late Quaternary slip rate and earthquake potential of marine reverse faults along the North Westland deformation front, New Zealand: New Zealand Journal of Geology and Geophysics: Vol 59, No 1

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Figure S4.

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Figure S3. Interpretation of major late Quaternary faults and associated anticlinal folds offshore of Kahurangi Point and Whanganui Inlet.

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Figure S2. Map showing details of Cape Foulwind Fault segmentation west of Kongahu Point.

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Figure S1.

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Table S1. Earthquake source parameters, offshore Westland, defined using the method of Stirling et al. (2012).

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Structure, late Quaternary slip rate and earthquake potential of marine reverse faults along the North Westland deformation front, New Zealand

Figure S4.

Figure S3. Interpretation of major late Quaternary faults and associated anticlinal folds offshore of Kahurangi Point and Whanganui Inlet.

Figure S2. Map showing details of Cape Foulwind Fault segmentation west of Kongahu Point.

Figure S1.

Table S1. Earthquake source parameters, offshore Westland, defined using the method of Stirling et al. (2012).

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Structure, late Quaternary slip rate and earthquake potential of marine reverse faults along the North Westland deformation front, New Zealand

Figure S4.

Figure S3. Interpretation of major late Quaternary faults and associated anticlinal folds offshore of Kahurangi Point and Whanganui Inlet.

Figure S2. Map showing details of Cape Foulwind Fault segmentation west of Kongahu Point.

Figure S1.

Table S1. Earthquake source parameters, offshore Westland, defined using the method of Stirling et al. (2012).

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